| RICO (clouds & climate processes) |
| Scanning, Scanning ... one of the principal instruments during RICO was the scanning S- and Ka- band radars, known as SPolka. Our analysis of their data is targeted to better understand the spatial and temporal distribution of rain during the field project, its relationship to cloud coverage and other macroscopic aspects of the lower troposphere. | ||
Description of scanning strategy:
|
||
![]() |
Preliminary analysis at UCLA has focused on quantifying surface rain rates using filtered surveillance scan, and other data. An example of this analysis is shown on the left where a sample unfiltered and filtered surveillance scan is shown as well as a rain-rate time-series showing rain rates and echo coverage from the S-Pol data, with estimates from TRMM, GPCP and surface measurements at Barbuda superimposed. This analysis is preliminary and will be revised, but for those interested in getting a feel for the preliminary data, it is provided here. The analysis of this preliminary data set has been conducted by Louise Nuijens and is described in her master thesis. TRMM overpass times are listed here. In some cases the circles appear to terminate a few seconds shy of 1800s, which means that the end points of each circle should be examined critically if velocity data (which is sensitive to sharp changes in pitch and roll) is to be used along a circle. |
|
Radar Links
Disclaimer: These data are a preliminary research product and subject to change. Although our ongoing syntheses are made available to all, we ask that their use be coordinated with the PI and Ms. Louise Nuijens. The original data from which these syntheses have been constructed are the authoritative data set and are publically available on the RICO archive. |
||